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碳酸化磷灰石在锶溶液存在下的亚稳平衡溶解行为。

Metastable equilibrium solubility behavior of carbonated apatite in the presence of solution strontium.

作者信息

Heslop D D, Bi Y, Baig A A, Higuchi W I

机构信息

Department of Pharmaceutics and Pharmaceutical Chemistry, 213 A Skaggs Hall 30 S 2000 E, University of Utah, Salt Lake City 84112, USA.

出版信息

Calcif Tissue Int. 2004 Jan;74(1):72-85. doi: 10.1007/s00223-002-0035-8. Epub 2003 Nov 26.

Abstract

The purpose of this study was to use the concept of metastable equilibrium solubility (MES) to describe the anomalous solubility behavior of carbonated apatite (CAP) in the presence of solution strontium. A CAP sample (4.8 wt% CO(3), synthesized at 70 degrees C) was prepared by precipitation. Baseline MES distributions were determined in a series of 0.1 M acetate buffers containing only calcium and phosphate (no strontium) over a broad range of solution conditions. In order to assess the influence of strontium, MES profiles were then determined in a similar fashion with 20, 30, 40, 50, 60, 70, and 80% of the solution calcium being replaced on an equal molar basis by solution strontium. From the compositions of the equilibrating buffer solutions, ion activity products (IAPs) of the form Ca(10-n)Sr(n)(PO(4))(6)(OH)(2) (n = 0-10) were calculated in an attempt to determine the correct function governing the dissolution of the CAP preparation. The results demonstrate the following important findings: (a) at high solution strontium/calcium ratios (i.e., when 60% or more of the solution calcium was replaced by strontium), the MES profiles in all the experiments were found to be essentially superimposable when the solution IAPs were calculated using the stoichiometry of Ca(6)Sr(4)(PO(4))(6)(OH)(2), and (b), at low solution strontium/calcium ratios (i.e., when 40% or less of the solution calcium was replaced by strontium), the stoichiometry yielding MES data superpositioning was found to be that of hydroxyapatite. When other stoichiometries were assumed, good superpositioning of the data was not possible.

摘要

本研究的目的是利用亚稳平衡溶解度(MES)的概念来描述碳酸化磷灰石(CAP)在溶液中存在锶时的异常溶解行为。通过沉淀法制备了一个CAP样品(4.8 wt% CO(3),在70℃下合成)。在一系列仅含有钙和磷酸盐(无锶)的0.1 M醋酸盐缓冲液中,于广泛的溶液条件下测定了基线MES分布。为了评估锶的影响,随后以类似方式在溶液中20%、30%、40%、50%、60%、70%和80%的钙被等摩尔的锶取代的情况下测定了MES曲线。根据平衡缓冲溶液的组成,计算了Ca(10 - n)Sr(n)(PO(4))(6)(OH)(2)(n = 0 - 10)形式的离子活度积(IAPs),试图确定控制CAP制剂溶解过程的正确函数。结果表明了以下重要发现:(a)在高溶液锶/钙比时(即当溶液中60%或更多的钙被锶取代时),当使用Ca(6)Sr(4)(PO(4))(6)(OH)(2)的化学计量计算溶液IAPs时,所有实验中的MES曲线基本可叠加;(b)在低溶液锶/钙比时(即当溶液中40%或更少的钙被锶取代时),发现产生MES数据叠加的化学计量是羟基磷灰石的化学计量。当假设其他化学计量时,数据无法实现良好的叠加。

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